continental slope
A mountain ridge that separates the heads of opposing glacial valleys is called an arete. It is a narrow and sharp ridge formed by the erosive action of glaciers on both sides.
The Brazilian highlands end with a sharp drop down to the Atlantic coastal plain which forms a steep cliff called the Serra do Mar (Sea Ridge). This geographical feature spans along the southeastern coast of Brazil and rises abruptly from the coastal plain.
Jagged ridges that form on mountains are called "knife-edge ridges" or simply "knife ridges." These ridges are narrow, sharp, and often dangerous to traverse due to their steep drop-offs on either side. They require expert mountaineering skills to navigate safely.
The sharp features of the mountain were carved primarily through the process of erosion, where wind, water, and ice gradually wear down the rock surface over millions of years. Additionally, tectonic forces such as faulting and folding can also contribute to the creation of sharp mountain features.
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continental slope
A sharp drop-off beyond the continental shelf is called a continental slope. The continental slope marks the transition between the continental shelf and the deep ocean floor.
The sharp end of a pencil is called the "point."
an a flat only can be called an a flat There is no double sharp equivalent, but it is the same as G sharp.
what is a line with many sharp turns
Mainly no they do not, because they rarely eat coral as it is sharp and occasionally poisonous.
The last sharp in the circle of fifths is a B#.
no, g sharp is the only "landlocked" note, which means it can only be called g sharp or a flat, not any double sharps or double flats.
A note which is neither sharp nor flat is called natural.A natural
A sharp metal piece is typically called a "metal shard" or a "metal splinter."
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The sharp drop from the continental shelf to the continental rise is called the continental slope. This transition zone marks the boundary between the relatively shallow waters of the continental shelf and the deeper ocean floor. The slope typically features steep gradients and can be characterized by various geological formations and sediment deposits.